Climate risk in Davao City
Davao Region, Philippines
Main risks in Davao City
On earthquakes, Davao City ranks above at least 94% of the world's 626 large cities. Its storm winds, about 107 km/h once in 100 years, stay below hurricane force, though higher than in 84% of large cities. [2]
- Earthquakes
- severe shaking on firm ground (0.38 g), more on soft ground [1]
- Higher than 94% of the world's large cities; 3rd of 4 large cities in the Philippines.
- For comparison: Tehran 0.41 g, Santiago 0.4 g, Nagoya 0.39 g.
- g is the pull of gravity: from about 0.1 g, shaking is strong and can cause light damage to buildings.
0.38 g Natural Earth Earthquake shaking on firm ground, 10% chance in 50 years
This week in Davao City
This week's forecast risk around the city, by day and by hour, and the hazard events near it now. [3] [4] [5]
This week's forecast for the city cannot be shown here right now.
Open the city on the mapThe Earth right now
The Earth's pulse reads the whole world, not this city, so it is the same on every city's page.
Earth's pulse, from 0 to 100. It rises with the number of people in the path of disasters now under way; 90 matches the 2004 tsunami.
Open the live mapWhere else Davao City stands out
every night of the year
Tropical nights in 2025, over 20 °C [6]
Higher than 93% of the world's large cities; 1st of 4 large cities in the Philippines.
For comparison: Bangkok 337 nights, Mumbai 319 nights, Yangon 315 nights.
Davao City's climate in the 2050s
2041-2060 compared with 1991-2020, if emissions level off [7] [8]
By the 2050s, Davao City is projected to have the climate that Kuala Lumpur (Malaysia) has today.
+1.0 °C
Mean temperature over the year
+1.0 °C
Average daily high, warmest month
+1.0 °C
Average nightly low, coldest month
+1%
Precipitation over the year
If emissions keep rising, Kuala Lumpur (Malaysia) comes closest, though the match is only partial.
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Climates are compared on seasonal temperature and rainfall alone, each difference weighed against the city's usual swings from year to year (the method of Mahony et al. 2017); heat waves, the heat of city streets and the rising sea are left out. All 3 estimates from the climate models, the middle one and the two ends of their range, point to Kuala Lumpur. [9]
Everything else measured
From the highest among the world's 626 large cities to the lowest.
| Reading | Davao City | Among 626 large cities | Rank in the Philippines (1 = highest) |
|---|---|---|---|
| Sea level rise by 2050 over the 1995-2014 average, if emissions level off [10] | 21 cm, 15 cm of it after 2020 | higher than 52% of large coastal cities | Rank in the Philippines (1 = highest): 3 of 4 |
| Drought risk [11] | High | the same grade as 44% of large cities; higher than 50%, lower than 6% | |
| Days with 20 mm of rain or more in 2025 [6] | 9 days | higher than 48% of large cities | Rank in the Philippines (1 = highest): 4 of 4 |
| Warming by 2050, if emissions level off [8] | +1.9 °C | higher than 44% of large cities | Rank in the Philippines (1 = highest): 1 of 4 |
| Hottest day of 2025 [6] | 30.7 °C | higher than 10% of large cities | Rank in the Philippines (1 = highest): 4 of 4 |
| Water stress [11] | Low: under 10% of the available water drawn | lowest grade, like 30% of large cities | |
| Hot days in 2025, over 35 °C [6] | 0 days | like 37% of large cities | |
| River flood depth, 100-year event [12] | Dry at the centre; other districts can flood | like 85% of large cities | |
| Share of the land around the centre (a 10 km square) that a 100-year flood from the sea puts under 0.5 m of water or more [12] | 0% today and by 2080 if emissions keep rising | like 74% of large coastal cities | |
| Share of land sinking over 1 cm a year, within 15 km [13] | 0% | like 80% of large cities | |
| Land burned in an average year [14] | 0% | like 84% of large cities |
- Flood depth is given for one 1 km square at the city centre, in today's climate.
- Land subsidence comes from a model of satellite radar measurements from 2013 to 2019 in 2 km squares, read over all the land within 15 km of the centre rather than at one point.
- Water stress is the share of the available water drawn every year. Drought risk is how often droughts come, against the area's own usual rain, and how many people and how much farmland they would reach. Both are graded on WRI's own scale.
- Sea level rise is the IPCC projection for the nearest coast, counted from the 1995-2014 average. It is on a grid about 100 km across and counts the slow rise or fall of the land. "If emissions level off" is the IPCC's SSP2-4.5 scenario.
- Water stress and drought risk have no rank in the country: they are steps of a scale, and many cities share one.
- Tsunamis and landslides are not rated for a single city here.
The nearest large cities
Distance from centre to centre.
- Cagayan de Oro · Philippines · 180 km
- Manila · Philippines · 980 km
- Quezon City · Philippines · 980 km
- Makassar · Indonesia · 1,530 km
Large cities in the Philippines
Sources
- GSHAP Global Seismic Hazard Map: earthquake shaking
- IRIS: the Imperial College Storm Model dataset: tropical cyclone wind
- Environment and Climate Change Canada: Global Deterministic Prediction System (GDPS): the week's forecast map
- EMSC-CSEM SeismicPortal: earthquake near the city now
- NASA Fire Information for Resource Management System (FIRMS): wildfire near the city now
- ERA5 Single Levels Daily Statistics: nights, heavy rain, hottest day, hot days
- TerraClimate: the 2050s comparison
- NASA Earth Exchange Global Daily Downscaled Projections (NEX-GDDP-CMIP6): the 2050s comparison, warming
- Mahony, Cannon, Wang and Aitken (2017). A closer look at novel climates: new methods and insights at continental to landscape scales. Global Change Biology 23, 3934-3955: how climates are compared
- IPCC AR6 Sea Level Projections: sea level rise
- Aqueduct 4.0 Water Risk Framework: drought risk, water stress
- Aqueduct Floods Hazard Maps: river flood depth, coastal floods
- Global Land Subsidence Mapping Reveals Widespread Loss of Aquifer Storage Capacity: sinking land
- Global Biomass Burning at 500 m (GFED500): burned land
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In a line
Source: Criora (criora.com), based on GSHAP, IRIS, ECCC, EMSC-CSEM SeismicPortal, NASA Fire Information for Resource Management System (FIRMS), ECMWF, TerraClimate, NEX-GDDP-CMIP6, IPCC, WRI, HydroShare, GFED500
APA
Criora. (2026). Davao City, Philippines: climate risk profile [Data set]. Retrieved November 4, 2026, from https://criora.com/atlas/PHL/davao-city BibTeX
@misc{criora_atlas_PHL_davao_city_2026,
author = {{Criora}},
title = {Davao City, Philippines: climate risk profile},
year = {2026},
url = {https://criora.com/atlas/PHL/davao-city},
urldate = {2026-11-04}
} The figures may be reused on the terms of their sources, which this page names.
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